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Dayton Limestone

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Series: GSA Field Guide
Published: 01 January 2012
DOI: 10.1130/2012.0027(05)
EISBN: 9780813756271
... Courthouse, Dayton, Ohio. Front entrance viewed from Main Street. Note that the entire exterior of the building is made of Dayton limestone. The capitals on the columns are based on the Ionic order. The building is located on the NW corner of Main Street and Third Street and is the historic center of Dayton...
FIGURES | View All (35)
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1964
AAPG Bulletin (1964) 48 (4): 543–544.
... thinner, and only a thin wedge of the lower part extends into southernmost Ohio. Here this lower unit is overlain by the Dayton limestone, which underlies a shale sequence called the Alger formation in Ohio. The Alger is a northern extension of the Estill clay. Zone I is represented in the Kankakee...
Series: GSA Field Guide
Published: 01 January 2012
DOI: 10.1130/2012.0027(04)
EISBN: 9780813756271
...; locally argillaceous. Osgood Shale 6.2–8.1 (1) Bluish gray to gray shale; calcareous; contains sparse, thin to massive interbeds of limestone and dolomite. Dayton Limestone 3.8 (1) Gray to bluish gray limestone; fine grained; mostly in medium to thick beds; dolomitic. Brassfield...
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Journal Article
Journal: GSA Bulletin
Published: 01 November 1948
GSA Bulletin (1948) 59 (11): 1121–1164.
... the Brazer formation, are 3700 feet thick at one locality in the quadrangle, a much more complete exposure than at the type locality of the formation in the Randolph quadrangle to the east. Pennsylvanian rocks reach a total thickness of 6000 feet in this area. A stromatolitic limestone in the Wasatch...
Series: GSA Field Guide
Published: 01 January 2012
DOI: 10.1130/2012.0027(06)
EISBN: 9780813756271
.... Sculpture measures 2.5 × 4.75 ft (0.76 × 1.45 m) ( Hansen, 1990 ). Photograph by M. Sandy. Abstract This field trip will be to a working limestone quarry near Paulding, Paulding County, Ohio, a little over 100 mi (160 km) north of Dayton, Ohio. The quarry is working Middle Devonian strata...
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Series: GSA Special Papers
Published: 01 January 1991
DOI: 10.1130/SPE258-p29
... The Old Kentucky River system was a major contributor to the Teays River, draining southwestern Ohio and much of eastern Kentucky. The trunk river flowed northward from southeastern Kentucky throughout Frankfort and Carrollton, and then past Cincinnati and Dayton, joining the Teays River near...
Series: AAPG Special Publication
Published: 01 January 1926
DOI: 10.1306/SV1328C26
EISBN: 9781629812601
... Abstract The South Dayton-Liberty salt dome is a characteristic Gulf Coast salt dome. The salt core is 1½ by 2½ miles in diameter and comes to within 500 feet of the surface. The major diameter strikes N. 30° E. The cap is 150–250 feet thick and consists of gypsum and anhydrite with a thin...
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1925
AAPG Bulletin (1925) 9 (3): 655–666.
...W. F. Bowman ABSTRACT The South Dayton-Liberty salt dome is a characteristic Gulf Coast salt dome. The salt core is 1 1 2 by 2 1 2 miles in diameter and comes to within 500 feet of the surface. The major diameter strikes N. 30° E. The cap is 150–250 feet thick and consists of gypsum and anhydrite...
FIGURES | View All (5)
Image
—<span class="search-highlight">Limestone</span> bed and thin-section photomicrograph. A = sandy fossiliferous li...
Published: 01 July 1984
Figure 9 —Limestone bed and thin-section photomicrograph. A = sandy fossiliferous limestone with dark mudstone rip-up clasts (Dayton Canyon). B = sandy biosparrudite showing shell fragments cut by quartz veins.
Journal Article
Journal: Geosphere
Published: 01 December 2016
Geosphere (2016) 12 (6): 1813–1832.
... units. Furthermore, the Wolcott Limestone has a gradational lower contact with the underlying Sodus Shale, both of which are progressively truncated to the west by a regionally angular unconformity at the base of S-IV ( Gillette, 1947 ; Brett et al., 1990 , 1998 ). The base of the Dayton Formation...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1917
AAPG Bulletin (1917) 1 (1): 34–59.
.... The upper surface of the salt deposits appear to be somewhat irregular. At Anse La Butte the top of the salt is separated from the main body by several feet of gravel. At South Dayton it comes in contact with a hard limestone. At Dayton the upper portion is mixed with sand and the same condition exists...
Journal Article
Published: 01 March 2015
Journal of Paleontology (2015) 89 (2): 245–256.
..., Temnocrinus americanus n. sp. Temnocrinus was previously recognized only from the Much Wenlock Limestone (Homerian) of England. The richness of this crinoid fauna from Bath County is low in comparison to that from the Dayton, Ohio, area, but crinoids, rhombiferans...
FIGURES
Journal Article
Published: 01 September 1927
Bulletin of the Seismological Society of America (1927) 17 (3): 129–136.
.... Geological Survey , Professional Paper 51 , 1906 ; U.S. Geological Survey , Geologic Atlas, Bald Mountain-Dayton folio , No. 141 , 1906 ; U.S. Geological Survey , Geologic Atlas, Cloud Peak-Fort McKinney folio , No. 142 , 1906 . 3...
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1940
AAPG Bulletin (1940) 24 (4): 672–692.
... of calcareous shale, calcareous dolomite and limestone. The general thickness ranges from 120 to 200 feet with an average of about 150 feet. The recognized units in ascending order are Brassfield limestone, Dayton dolomite, and Alger shale with a thin dolomite, Laurel, in the upper part. The Alger shale...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1942
AAPG Bulletin (1942) 26 (2): 162–187.
.... The formation was first distinguished as a separate stratigraphic unit by Packard (7, p. 140), who named it from Trabuco Canyon. It is a soft red deeply weathered massive conglomerate composed of an unsorted mass of cobbles including in its composition metamorphosed sandstones, cherts, limestones, and slates...
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Journal Article
Published: 11 May 2020
Journal of Sedimentary Research (2020) 90 (5): 449–467.
... microbial activity. These factors allow interstitial waters to remain weakly supersaturated with respect to aragonite. Comparison with Permian analogs indicates that lithification is delayed until deposits reach burial depths at which chemical compaction proceeds. The ultimate end product is limestone...
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Journal Article
Published: 01 March 2023
Journal of Paleontology (2023) 97 (2): 380–385.
...), Indiana (Frest et al., 1999 ); the Welton Member of the Scotch Grove Formation (Telychian–Wenlock), Iowa; Wolcott Limestone (Telychian), New York (Eckert and Brett, 2001 ); and the lower Visby Formation (Telychian), Sweden (Angelin, 1878 ). Of these diverse Llandovery echinoderm faunas, only the Cybele...
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